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121.
Luo Dehai 《Acta Meteorologica Sinica》1992,6(3):390-394
Introducing the concept of pseudo-momentum, a generalized Arnold-Dikii functional is established, and then thesufficient condition for stability of nonlinear wave motion in the barotropic nondivergent atmosphere is derived by useof variational principle. It is found that the stability of nonlinear wave motion depends not only on its streamfield distri-bution, but also on its phase speed for the propagating nonlinear wave motion. Moreover, the stability criterion of trav-elling modon is also obtained, and it is shown that the travelling modon is stable if the scale of disturbance superimposedon the travelling modon remains to be less than that of the travelling modon. 相似文献
122.
In this study, we analyzed 1979–2019 daily ERA-Interim reanalysis data in winter and performed atmospheric circulation experiments to examine the modulation of Arctic sea ice in western Greenland(Baffin Bay, Davis Strait, and the Labrador Sea, BDL) on winter Greenland blockings. It is found that low BDL sea ice and high BDL surface temperature favor frequent, long-lived, westward-moving Greenland blockings in winter, which cause frequent and strengthening cold surges over the mid-eastern United States. In contrast, high BDL sea ice and low BDL surface temperature favor short-lived, less frequent and quasi-stationary Greenland blockings, mainly leading to cold anomalies in North Europe. Low wintertime BDL sea ice reduces the background potential vorticity meridional gradient(PVy) and zonal wind over the mid-high latitudes of the North Atlantic, which enhances the nonlinearity of Greenland blocking, accelerates the phase speed of its westward movement, and weakens its energy dispersion, thus favoring the occurrence and persistence of Greenland blocking. High BDL sea ice strengthens the background PVyand zonal wind in the mid-high latitudes of the North Atlantic, which weakens the nonlinearity and movement of Greenland blocking, enhances its energy dispersion, and thus suppresses the occurrence and persistence of Greenland blocking and its retrogression. A set of atmospheric circulation experiments supports the above results based on the reanalysis dataset. 相似文献
123.
旋转正压大气中的Rossby孤立波和偶极子阻塞 总被引:1,自引:0,他引:1
大气中的阻塞动力学一直是大气动力学中所要解决的重要问题之一,随着数学的发展,阻塞动力学的研究也取得了较大的进展.大气中的阻塞可以分为两类:一类是单个非偶极子阻塞(只存在高压或低压),另一类是偶极子阻塞(高压的南侧存在闭合的低压).关于偶极子阻塞的动力学研究是在80年代以后才进行的.为了解释大气中所出现的偶极子阻塞,Mcwilliams[1](1980)提出了Equivalent Modon理论,在他的理论中,他强调了辐散效应的作用.随后Shutt[2](1983)指出通过湍涡的强迫作用在大气中可以形成偶极子阻塞,但这些理论均不能反映偶极子阻塞的形成过程,这以后Malguzzi和Malanotte-Rizzoli[3-4](1984,1985)提出T用Rossby孤立波来解释大气中偶极子阻塞的形成过程.但上面所提出的理论不能解释偶极子阻塞的崩溃过程.作者[5](1989)提出了用包花络Rossby孤立波理论来描述大气中偶极子阻塞的形成、维持和崩溃过程,由于偶极子阻塞随纬度具有不同的分布,这个问题远没解决,本文的目的在于使用旋转正压大气中的Rossby孤立波来探讨偶极子阻塞的纬度分布. 相似文献
124.
文章分析秦皇岛4个海水浴场6个监测站位2015—2018年采集水质样品中粪大肠菌群和溶解氧的变化趋势,并结合《海水水质标准》和《海滨浴场游泳适宜度分级规定》,对4个浴场的水质进行分析评价。结果表明:粪大肠菌群是海水浴场的主要污染物,粪大肠菌群浓度的变化主要受降雨、游客数量、温度和陆源污染物影响。尤其强降雨后,粪大肠菌群浓度升高较明显。浴场的溶解氧含量变化不大,年均值均满足二类水质标准,其主要受水温和浮游生物等因素影响,高峰值多出现在9月和10月。秦皇岛4个海水浴场的水质优良状况表现为南戴河浴场最好、东山浴场和北戴河浴场次之、西浴场最差。 相似文献
125.
126.
1.IntroductionSincethe40--50--dayoscillationinthetropicalPacificwasfirstfoundbyMaddenandJulian(1971,1972),ithaslongbeenanimportantresearchtopic.Inobservationalstudies,LauandChan(1985,1986),GhilandMo(1991)showedthattheintraseasonaloscillationsinthetro... 相似文献
127.
128.
Eight known compounds were isolated from a marine-derived bacterium Streptoverticillium luteoverticillatum 11014 using bioassay-guided fractionations. Their structures were identified by spectral analysis as bis (4-hydroxybenzyl) ether (1), p-hydroxyphenylethyl alcohol (2), N-(4-hydroxyphenethyl) acetamide (3), indole-3 carboxylic acid methyl ester (4), dibenzo[b,e] [1,4]dioxine (5), thymine (6), cytosine deoxyribonucleoside (7) and 2, 3-butanediol (8). These compounds were evaluated for their cytotoxic activities against K562 cell line with the SRB method for the first time. Compounds 2 and 4 showed cytotoxcities with IC50 values of 101.1 and 165.3 μmolL-1, respectively. All compounds were isolated from S. luteoverticillatum 11014 for the first time. 相似文献
129.
1. IntroductionIn the mid--high latitudes, l' blocking flow" is an importaht part of the low--frequency variability of the atmospheric circulation. Owing to its longevity and large amplitude, a blocking flow configuration can usually cause prolonged anomalous weather situations over certain extratropical regions. Therefore, it has been a primary interest of many synoptic anddynamical meteorologists. In the past decades, the interaction of planetary waves with migratory, synoptic--scale waves h… 相似文献
130.